Peterson Michael, Rudlosky Scott, Deierling Wiebke
Cooperative Institute for Climate and Satellites-Maryland, Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD, USA.
NOAA/NESDIS/STAR, College Park, MD, USA.
J Geophys Res Atmos. 2018 Sep 16;123(17):9674-9687. doi: 10.1029/2018JD028583.
Optical lightning measurements from the Lightning Imaging Sensor (LIS) are used to map the lateral development of lightning flashes and produce statistics that describe their motion through the electrified cloud. This is accomplished by monitoring the frame-by-frame (group-level) evolution of the optical signals produced during each flash. While the optical flash properties recorded by LIS gravitate towards the most exceptional optical signals produced during the flash, group-level data describe the evolution and lateral development of the flash resulting from physical lightning process that emits enough light out of the top of the cloud to be detected from orbit. The groups that comprise LIS flashes constitute examples of complex lateral flash structure that can extend 80 km in length with dozens to hundreds of visible branches. The lateral development of individual flashes is described in terms of its speed and direction of motion, whether the development extends the overall length of the flash or reilluminates an existing segment, and whether it is directed inbound or outbound with respect to the origin. Sixty-five percent of propagating groups are directed outbound from the origin, 22% extend the length of the flash, and 3-5% reilluminate an existing branch. LIS flashes are commonly oriented from east to west and develop at speeds ranging from 10 to 10 m/s, consistent with large-scale leader development. These results provide evidence that lightning imagers may be used in conjunction with Lightning Mapping Array systems to document physical lightning phenomena across global domains.
闪电成像传感器(LIS)的光学闪电测量数据用于绘制闪电回击的横向发展情况,并生成描述其在带电云层中移动的统计数据。这是通过监测每次闪电过程中产生的光信号逐帧(组级)演变来实现的。虽然LIS记录的光学闪电特性倾向于闪电过程中产生的最特殊的光信号,但组级数据描述了闪电的演变和横向发展情况,这种闪电是由物理闪电过程产生的,该过程从云层顶部发出足够的光,以便从轨道上被探测到。构成LIS闪电的组是复杂横向闪电结构的示例,其长度可延伸80公里,有数十到数百个可见分支。单个闪电的横向发展是根据其移动速度和方向来描述的,即发展是延伸了闪电的总长度还是重新照亮了现有部分,以及它相对于起点是向内还是向外移动。65%的传播组是从起点向外移动的,22%延伸了闪电的长度,3 - 5%重新照亮了现有分支。LIS闪电通常从东向西定向,发展速度在10到10米/秒之间,这与大规模先导发展一致。这些结果证明,闪电成像仪可与闪电定位阵列系统结合使用,以记录全球范围内的物理闪电现象。